{"@context":{"obo_purl":"http://purl.obolibrary.org/obo/","rdf":"http://www.w3.org/1999/02/22-rdf-syntax-ns#","owl":"http://www.w3.org/2002/07/owl#","rdfs":"http://www.w3.org/2000/01/rdf-schema#","skos":"http://www.w3.org/2004/02/skos/core#","oboinowl_gen":"http://www.geneontology.org/formats/oboInOwl#","metadata_def":"http://data.bioontology.org/metadata/def/"},"@id":"obo_purl:ENVO_00002250","@type":"owl:Class","rdfs:subClassOf":{"@id":"obo_purl:ENVO_00001998"},"rdfs:label":"plinthosol","skos:notation":"ENVO:00002250","obo_purl:IAO_0000115":"Plinthosols are soils with plinthite, petroplinthite or pisoliths. Plinthite is an Fe-rich (in some cases also Mn-rich), humus-poor mixture of kaolinitic clay (and other products of strong weathering such as gibbsite) with quartz and other constituents that changes irreversibly to a layer with hard nodules, a hardpan or irregular aggregates on exposure to repeated wetting and drying. Petroplinthite is a continuous, fractured or broken sheet of connected, strongly cemented to indurated nodules or mottles. Pisoliths are discrete strongly cemented to indurated nodules. Both petroplinthite and pisoliths develop from plinthite by hardening.","oboinowl_gen:hasOBONamespace":"ENVO","oboinowl_gen:id":"ENVO:00002250","oboinowl_gen:inSubset":{"@id":"obo_purl:ENVO_03605015"},"metadata_def:prefLabel":"plinthosol","metadata_def:mappingLoom":"plinthosol","metadata_def:mappingSameURI":{"@id":"obo_purl:ENVO_00002250"}}
{"@context":{"obo_purl":"http://purl.obolibrary.org/obo/","rdf":"http://www.w3.org/1999/02/22-rdf-syntax-ns#","owl":"http://www.w3.org/2002/07/owl#","rdfs":"http://www.w3.org/2000/01/rdf-schema#","skos":"http://www.w3.org/2004/02/skos/core#","oboinowl_gen":"http://www.geneontology.org/formats/oboInOwl#","metadata_def":"http://data.bioontology.org/metadata/def/"},"@id":"obo_purl:ENVO_00002250","@type":"owl:Class","rdfs:subClassOf":{"@id":"obo_purl:ENVO_00001998"},"rdfs:label":"plinthosol","skos:notation":"ENVO:00002250","obo_purl:IAO_0000115":"Plinthosols are soils with plinthite, petroplinthite or pisoliths. Plinthite is an Fe-rich (in some cases also Mn-rich), humus-poor mixture of kaolinitic clay (and other products of strong weathering such as gibbsite) with quartz and other constituents that changes irreversibly to a layer with hard nodules, a hardpan or irregular aggregates on exposure to repeated wetting and drying. Petroplinthite is a continuous, fractured or broken sheet of connected, strongly cemented to indurated nodules or mottles. Pisoliths are discrete strongly cemented to indurated nodules. Both petroplinthite and pisoliths develop from plinthite by hardening.","oboinowl_gen:hasOBONamespace":"ENVO","oboinowl_gen:id":"ENVO:00002250","oboinowl_gen:inSubset":{"@id":"obo_purl:ENVO_03605015"},"metadata_def:prefLabel":"plinthosol","metadata_def:mappingLoom":"plinthosol","metadata_def:mappingSameURI":{"@id":"obo_purl:ENVO_00002250"}}